中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Saline rhythm and climatic change since 20.6 kyr BP from the Qiulinanmu Playa Lake in Tibet

文献类型:期刊论文

作者Fang XM(方小敏); Kang SC(康世昌)
刊名CARBONATES AND EVAPORITES
出版日期2010
卷号25期号:1页码:5-14
关键词GULIYA ICE CORE LACUSTRINE SEDIMENTS STABLE ISOTOPES ASIAN MONSOON HOLOCENE PLATEAU CHRONOLOGY CHINA FRACTIONATION GEOCHEMISTRY
通讯作者康世昌
合作状况其它
学科主题自然地理学
收录类别SCI
语种英语
WOS记录号WOS:000279006900002
公开日期2011-04-28
源URL[http://ir.itpcas.ac.cn:8080/handle/131C11/1405]  
专题青藏高原研究所_图书馆
推荐引用方式
GB/T 7714
Fang XM,Kang SC. Saline rhythm and climatic change since 20.6 kyr BP from the Qiulinanmu Playa Lake in Tibet[J]. CARBONATES AND EVAPORITES,2010,25(1):5-14.
APA Fang XM,&Kang SC.(2010).Saline rhythm and climatic change since 20.6 kyr BP from the Qiulinanmu Playa Lake in Tibet.CARBONATES AND EVAPORITES,25(1),5-14.
MLA Fang XM,et al."Saline rhythm and climatic change since 20.6 kyr BP from the Qiulinanmu Playa Lake in Tibet".CARBONATES AND EVAPORITES 25.1(2010):5-14.

入库方式: OAI收割

来源:青藏高原研究所

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